By analyzing the physical geography, regional hydrology and geology information, and groundwater equilibrium of DunHuang Basin, this paper simulates the aquiferous layer which has the thickness of 250 m, and consider it as two dimension mixed layer which is heterosphere and isotropy.

  • 通过敦煌盆地自然地理和区域水文地质及盆地地下水均衡分析,将250m左右深度处稳定流线以上的含水层作为数值模拟对象,概化为非均质各向同性平面二维流混合层;

  • 互联网摘选 2025-01-19 23:26:06

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